Massive extraction of groundwater can resolve a puzzle over a rise in sea levels in past decades,scientists in Japan said today.

Global sea levels rose by an average of 1.8 millimetres (0.07 inches) per year from 1961-2003,according to data from tide gauges.

But the big question is how much of this can be pinned to global warming.

In its landmark 2007 report,the UN’s Nobel-winning Intergovernmental Panel on Climate Change (IPCC) ascribed 1.1mm (0.04 inches) per year to thermal expansion of the — water expands when it is heated — and to meltwater from glaciers,icecaps and the Greenland and Antarctica icecaps.

That left 0.7mm (0.03 inches) per year unaccounted for,a mystery that left many scientists wondering if the data were correct or if there were some source that had eluded everyone.

In a study published in the journal Nature Geoscience,a team led by Yadu Pokhrel of the University of Tokyo say the answer lies in water that is extracted from underground aquifers,rivers and lakes for human development but is never replenished.

The water eventually makes it to the ocean through rivers and evaporation in the soil,they note.

Groundwater extraction is the main component of additions that account for the mystery gap,according to their paper,which is based on computer modelling.

“Together,unsustainable groundwater use,artificial reservoir water impoundment,climate-driven change in terrestrial water storage and the loss of water from closed basins have contributed a sea-level rise of 0.77mm (0.031 inches) per year between 1961 and 2003,about 42 percent of the observed sea-level rise,” it says.

The probe seeks to fill one of the knowledge gaps in the complex science of climate change.

Researchers admit to many unknowns about how the oceans respond to warming,and one of them is sea-level rise,an important question for hundreds of millions of coastal dwellers.

Just a tiny rise,if repeated year on year,can eventually have a dramatic impact in locations that are vulnerable to storm surges or the influx of saltwater into aquifers or coastal fields.